Abstract
Sorption to the phyllosilicate clay minerals Illite, kaolinite, and bentonite has been studied for a wide variety of organic cations using a flow-through method with fully aqueous medium as the eluent. Linear isotherms were observed at concentrations below 10% of the cation-exchange capacity (CEC) for Illite and kaolinite and below 1 mmol/kg (
Original language | English |
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Pages (from-to) | 14224-14232 |
Number of pages | 9 |
Journal | Environmental Science and Technology |
Volume | 42 |
Issue number | 24 |
Publication status | Published - 2013 |